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Modelling the δ18O value of cave drip water and speleothem calcite

Stable isotope signals recorded in speleothems have provided important insights about past climate variability in recent years. Quantitative reconstruction of mean annual temperature and the amount of precipitation, however, remains difficult because the stable isotope signals are influenced by vari...

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Hauptverfasser: Wackerbarth, Anne Katrin (VerfasserIn) , Scholz, D. (VerfasserIn) , Fohlmeister, Jens (VerfasserIn) , Mangini, Augusto (VerfasserIn)
Dokumenttyp: Article (Journal)
Sprache:Englisch
Veröffentlicht: 12 October 2010
In: Earth and planetary science letters
Year: 2010, Jahrgang: 299, Heft: 3/4, Pages: 387-397
ISSN:1385-013X
DOI:10.1016/j.epsl.2010.09.019
Online-Zugang:Resolving-System, lizenzpflichtig, Volltext: https://doi.org/10.1016/j.epsl.2010.09.019
Verlag, lizenzpflichtig, Volltext: https://www.sciencedirect.com/science/article/pii/S0012821X10005947
Volltext
Verfasserangaben:A. Wackerbarth, D. Scholz, J. Fohlmeister, A. Mangini

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